1 / 9

A new unified boundary-layer scheme for RACMO: The DualM-TKE scheme

A new unified boundary-layer scheme for RACMO: The DualM-TKE scheme. Stephan de Roode with contributions from Geert Lenderink Roel Neggers Reinder Ronda Wim de Rooy Pier Siebesma Bert van Ulft Martin Koehler (ECMWF). EDMF: from fundamental turbulence studies to 3D RACMO simulations.

monte
Download Presentation

A new unified boundary-layer scheme for RACMO: The DualM-TKE scheme

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. A new unified boundary-layer scheme for RACMO: The DualM-TKE scheme Stephan de Roode with contributions from Geert Lenderink Roel Neggers Reinder Ronda Wim de Rooy Pier Siebesma Bert van Ulft Martin Koehler (ECMWF)

  2. EDMF: from fundamental turbulence studies to 3D RACMO simulations Large Eddy Simulation (LES) Models Cloud Resolving Models (CRM) Single Column Mode (SCM)l Versions of Climate Models 3d-Climate Models NWP’s 1. Design dualM-TKE scheme 2. SCM results for Cabauw 3. Outlook Time range for developing new scheme is more than 10 years

  3. The Eddy-Diffusivity Mass-Flux (EDMF) scheme • Nonlocal transport through strong updrafts in clear and cloudy boundary layer by advective Mass Flux (MF) approach • Remaining (local) transport done by an Eddy Diffusivity (ED) approach ED MF

  4. Advantages of EDMF • One updraft model for : dry convective BL, subcloud layer, cloud layer. • No trigger function for moist convection needed • No switching required between moist and dry convection needed • Easy and natural transition to neutral and stable PBL • Possible extension to deep convection Further Reading: Soares et al QJRMS (2004) Siebesma et al JAS (2007) De Rooy and Siebesma Accepted for MWR (2008) Neggers et al (submitted to JAS) Courtesy: Martin Kohler (ECMWF)

  5. Status Status EDMF • ECMWF model : Ready. Running in Test Suite. (Roel Neggers) • RACMO model: Ready. Will be used in next climate scenario runs (Stephan de Roode, Geert Lenderink) • Harmonie: Final checks in Single Column Model mode. 3D tests will start early 2008.(Wim de Rooy, Sylvie Malardel)

  6. Running Single Column Models (SCMs) for the Cabauw column - use RACMO 3D large-scale forcing for 2002-2003 - Run three SCM versions with RACMO 3D forcing ECMWF Cycle 31R1 Cycle 31 with dualM (future ECMWF version) RACMO dualM-TKE - Reset to RACMO3D profiles every 24 hours at 0000 UTC - differences in modeling results are due solely to differences in the turbulent transport schemes

  7. PDF LWP for low clouds only C31-R1 dualM-TKE C31-dualM

  8. Cloud base level PDFs C31-R1 dualM-TKE C31-dualM

  9. Outlook RACMO 3D • dualM-TKE has been implemented in 3D RACMO and is running • - compare cloud statistics with observations (CloudNet, MSG-SEVIRI) • - verify stable boundary layer structure, • e.g. Baas et al. (2008), parameterization test bed Roel Neggers • Simulate Hadley circulation (e.g. EUROCS Pacific case) • Clouds and radiation • - Consider implementation of new ECMWF Cycle 32 Monte-Carlo Independent Column Approximation (McICA) radiation scheme

More Related